“…This is probably due to those abundant inorganic minerals (i.e., Ca 2+ , Na + , K + , and Mg 2+ ) in the ash can exchange ions with Cd 2+ , finally generating coprecipitation and complexes. , The pH of biochar (ranging from 7 to 8.5) is found negatively correlated with the SHAP value (Figure e), which may be attributed to the presence of abundant functional groups (e.g., −COOH and −OH) that can strongly complex and stabilize Cd ions in soils. ,, However, this correlation becomes rather poor for the biochar pH higher than 8.5 ( R 2 = 0.047; Figure e). The elemental composition of biochar determines the type and quantity of surface functional groups of biochar; for instance, a higher O content of biochar leads to more abundant functional groups (such as −COOH), which can promote the chemical adsorption of Cd on biochar. Nevertheless, our SHAP analysis suggests that these variables of elemental compositions are poorly correlated to η-Cd (Figures f and S5b–d), implying that the key factors determining Cd immobilization may be not dominated by physicochemical processes …”